|Pond at Mount Allison University in Sackville, NB.|
Sunday, December 12, 2010
Friday, December 10, 2010
The vertical difference between high and low tide in the Bay of Fundy at Burntcoat Head, NS is about 17.0 m during the part of the month when the tidal range is most extreme. That's about the height of a 5 storey building! In places with a near flat beach, the difference between high and low tide points may be a kilometer or more. In a single tidal cycle of just over 12 hours, about 110 billion tons of water flows in and out of the Bay of Fundy. That sounds like a lot. To get a handle on just how much it is, it is equivalent to the combined total 24 hr flow of all the rivers of the world! It is not wonder that the Bay of Fundy is a finalist in the Seven Natural Wonders of the World.
What is the science of why the tidal range is so extreme in the Bay of Fundy, while most places the difference between high and low tide is just a meter or so. While it is the combined gravitational effects of the moon and the sun which produce tides anywhere, the reason they are particularly high here has to do with the physical dimensions of the bay. The most important effect is resonance - the tides are high in the Bay of Fundy because the size of the bay is just right to match the natural gravitational pushing cycle of the Moon that causes the tides.
Imagine you are pushing someone on a swing. The energy of the person on the swing is much more than you give them in any one push, but if you provide the push at just the right time, you keep building up the resonant response. In our case the swing is the flow of water in and out of the bay, and the push is provided by ocean tides caused in turn by the gravitational influence of the Moon mainly (another post will talk about tides in general).
There are two high tides a day, one when the ocean side is nearest the Moon, and one on the side of the Earth most distant from the Moon. This means that the tidal cycle is about 12 hr, but not exactly. That is because in a month the moon makes one orbit around the Earth, and therefore it takes a little more than 12 hr from one high tide to the next (about 12 hr and 25 minutes to be exact).
The Bay of Fundy is just the right length, about 270 km, for a resonance to exist, and we have a high tidal range response (like if you push the swing at just the right time, the person on the swing goes high). If the Bay of Fundy was a bit shorter, or a bit longer, the response would be less.
Many accounts on the web attribute the high tidal range to the shape of the bay. While it is true that the bay gets steadily narrower and shallower, and that helps push the water up, that is very much a secondary effect, with the size of the bay matching the resonant condition being more important. So the shape of the bay helps determine where the tidal range is highest, the fact we have higher tides in the Bay of Fundy region than elsewhere is primarily due to the size, not shape.
You (or your children) can experience this resonance for yourself in a model bay. Take a long pan with a bit of water in it. Try vibrating the pan with different frequencies (i.e. lift one end up and down in a regular way). If you do it really slowly, the water will just move more or less the amount you push the end of the pan up and down. If you do it really fast, not too much effect. But if you do it at just the right frequency, the sloshing back and forth will build up. And that building up, or resonance, is exactly what happens to create the high tides of the Bay of Fundy. If the bay were shorter, or longer, then there would not be a match, and the tidal range would be much less.
Now while the tidal range is always impressive, exactly how high the range will be is determined by astronomical and other factors. The spring tides (that have nothing to do with the season, but occur during times of full moon and new moon when Earth, Moon and Sun are in a line) will lead to the largest tidal range. Also, the Moon is closer to us sometimes and that will lead to a higher range (but that is a topic for another post!).
Monday, December 6, 2010
One of the rather unknown treasures of the Bay of Fundy, and one of my personal favourites, is Waterside Beach, located between Alma and Cape Enrage in New Brunswick. The water here is too cold for swimming, but this is a great place to enjoy the tidal range of the bay in a beautiful setting. The sand here seems to stretch forever in an almost flat beach, and best of all, the beach seldom has more than a handful of visitors, so you have the sense of a private beach. While the beach itself is very flat, it is defined by rocky outcroppings on both edges. The one nearer to Alma is a very interesting set of tide etched red rocks that can be explored at low tide. As always with rock outcroppings, avoid getting too near any vertical cliff.
Waterside Beach is easy to find: from the village of Alma (at the east entrance to Fundy National Park) take highway 915 which veers off to the right up the hill just after the Alma Baptist Church. After about 10 minutes driving from Alma you will see the beach. There is a small parking area on the right of the road, and then a short and easy walk gets you to the beach. If you plan on wading, the best time to visit the beach is just after low tide, when the incoming tide begins to cover the warmer sand. You truly get the sense of the tidal range if you stay in a spot and watch and feel the water as it comes in further each minute (the maximum rate of water height change will be half way between low and high tides. This is a great location for photographers, fun for kids, and a romantic location for couples. Don't miss it during your Bay of Fundy vacation!
Waterside Beach is one of the places listed on our Bay of Fundy vacation checklist. See the complete checklist at our Bay of Fundy website: bayfundy.net.